Synonyms of features appear indented below the primary name. The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Corcovado, probably of late-Pleistocene age, is eroded by glaciers and surrounded by Holocene cinder cones. Its only known historic activity was in 1834 and/or 1835. The volcano's base has likely prehistoric lava flows that are densely vegetated. The roughly 440-m-high volcano contains a 300 x 160 m wide crater. The town of Chaitén was formerly the main gateway to this protected area, but much of the town was destroyed by an eruption of Chaitén Volcano and the resultant mudflow in 2008. Corcovado Volcano is a stratovolcano located about 25 km south of the mouth of Yelcho River, in the Palena Province, Los Lagos Region, Chile. Corcovado Volcano Plate Boundary; Corcovado Volcano Climb; Entity Index This is the list of all entities in this result page. not at a plate boundary), such as the Hawaiian volcanoes within the Pacific Plate. Little is known of this isolated volcano that was seen in eruption by Darwin in 1834, and an eruption was reported to have occurred in November 1835. C. Darwin described seing it in activity in 1834 and an explosive eruption was reported to have occurred in November 1835 by a resident from Chiloe, 60 km west of the volcano. Little is known about Volcán Coronado and it is unknown when it last erupted. Corcovado volcano is an isolated and little studied stratovolcano in southern Chile. Click an entity to go directly to the entity box. MODIS looks at every square km of the Earth every 48 hours, once during the day and once during the night, and the presence of two MODIS sensors in space allows at least four hot-spot observations every two days. At its foot lies a series of lakes. The sharp-topped peak of Corcovado volcano rises above the Gulf of Corcovado as seen from the north from a helicopter near the town of Chaitén. If at least one is oceanic, it will subduct. The presence of a hot spot is inferred by anomalous volcanism (i.e. Each day updated global maps are compiled to display the locations of all hot spots detected in the previous 24 hours. Do you know this place? Corcovado Volcano is a stratovolcano located about 25 km south of the mouth of Yelcho River, in the Palena Province, Los Lagos Region, Chile. Smithsonian / USGS Weekly Volcanic Activity Report, Eruptions, Earthquakes & Emissions Application, Department of Mineral Sciences Rock and Ore collection, Incorporated Research Institutions for Seismology (IRIS), World Organization of Volcano Observatories (WOVO), Large Magnitude Explosive Volcanic Eruptions (LaMEVE), Volcano Global Risk Identification and Analysis Project (VOGRIPA), Integrated Earth Data Applications (IEDA), Corcobado | Jorobado | Chiloe, Volcan de (?). The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. Corcovado is ice-covered and basaltic to basaltic-andesite in composition. For each MODIS image, the algorithm automatically scans each 1 km pixel within it to check for high-temperature hot-spots. Corcovado Volcano Stratovolcano in Chile; 180° South 2010 film; Wiki Authority Control Authority control is a method of creating and maintaining index terms for bibliographical material in a library catalogue. If both are continental they will smash together and form a mountain range. Photo by Bryan Freeman, 2005. © TouristLink.com 2020, All Rights Reserved. The maps shown below have been scanned from the GVP map archives and include the volcano on this page. comm.). Eruptions in historical time were considered likely from these postglacial volcanoes (Moreno 1985, pers. The IAVCEI Commission on Volcanic Hazards and Risk has a, Middle InfraRed Observation of Volcanic Activity (. Here's the our members favorite photos of "Volcanoes in Quellon". Clicking on the small images will load the full 300 dpi map. The glacially eroded volcano is flanked by Holocene cinder cones. Corcovado Volcano (Spanish pronunciation: [koɾkoˈβaðo]) is a stratovolcano located about 25 kilometres (16 mi) south of the mouth of the Yelcho River, in the Palena Province, Los Lagos Region, Chile. The Global Volcanism Program has no Bulletin Reports available for Corcovado. There is no Emissions History data available for Corcovado. We welcome users to tell us if they see incorrect information or other problems with the maps; please use the Contact GVP link at the bottom of the page to send us email. Although the process is not clearly understood, magma apparently forms and rises by buoyancy from a depth of 100 to 200 km (60 to 120 miles). Upload your photo of Corcovado Volcano! EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility. The main edifice at Corcovado is likely Pleistocene in age, but historical eruptions have been reported, probably from Holocene cinder cones surrounding the volcano. The eruption has had serious consequences for the nearby town of Chaitén… The town of Chaitén was formerly the main gateway to this protected area. The volcano and the adjacent area form part of Corcovado National Park. Three tephra layers are linked to Corcovado volcano, of which the two youngest are dated 7,980 BP and 6,870 BP respectively. Hot spots also develop beneath continents. The maps database originated over 30 years ago, but was only recently updated and connected to our main database. The Global Volcanism Program has no Weekly Reports available for Corcovado. Chilean Continent. The glacially eroded volcano is flanked by Holocene cinder cones. The dramatic summit spire of Corcovado volcano is seen in this telephoto view from the west from the town of Quellon on the island of Chiloe. The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano. Using infrared satellite Moderate Resolution Imaging Spectroradiometer (MODIS) data, scientists at the Hawai'i Institute of Geophysics and Planetology, University of Hawai'i, developed an automated system called MODVOLC to map thermal hot-spots in near real time. Converging plates can be oceanic, continental, or one of each. Eruptions were reported in historical time from these flank cones. A series of lakes flank the eastern side of the basaltic to basaltic-andesite structure. When one is found the date, time, location, and intensity are recorded. The glacially eroded volcano is flanked by Holocene cinder cones. Corcovado Volcano (Spanish pronunciation: [koɾkoˈβaðo]) is a stratovolcano located about 25 kilometres (16 mi) south of the mouth of the Yelcho River, in the Palena Province, Los Lagos Region, Chile. A subducting plate creates volcanoes. Recreation / Outdoor near Corcovado Volcano. The Hawaiian hot spot has been active at least 70 million years, producing a volcanic chain that extends 3,750 miles (6,000 km) across the northwest Pacific Ocean. Gonzalez-Ferran O, 1995. Last eruption :     4920 BC ± 100. The light-colored delta at the left was formed by lahar deposition during the eruption of Chaitén volcano beginning in 2008. Volcanes de Chile. Corcovado dominates the landscape of the Gulf of Corcovado area and is visible from Chiloé Island, weather permitting. Make me an Ambassador. Grow your travel business and get new leads from interested customers. At its foot lies a series of beautiful lakes. Locations with converging in which at least one plate is oceanic at the boundary have volcanoes. The most distinctive feature of this volcano is its stepped top, similar to that of Puntiagudo Volcano.